TY - JOUR
T1 - Measurement of vertical liquid water path by means of an airborne radiometer and the shortwave albedo of marine low-level clouds during WENPEX in Japan
AU - Fujiyoshi, Y.
AU - Ishizaka, Y.
AU - Takeda, T.
AU - Hayasaka, T.
AU - Tanaka, M.
PY - 1995
Y1 - 1995
N2 - The result of the air truth of the LWPradiometer indicates that the 37-GHz microwave radiometer gives an estimation of the LWP accurate to 100 mg cm-2. The shortwave cloud albedo was related to the LWPradiometer. The albedo increases with the LWP, independent of cloud type, when measured just above the cloud tops. The measured albedo is nearly the same as the calculated albedo when the LWPradiometer is larger than 60 mg cm-2 but much smaller than the calculated albedo when the LWPradiometer is less than 40 mg cm-2. Cloud-top irregularity is suggested to be the primary cause of this discrepancy. The degree of inhomogeneity of the horizontal distribution of liquid water appears to be correlated with the amount of precipitable water in the planetary boundary layer. -from Authors
AB - The result of the air truth of the LWPradiometer indicates that the 37-GHz microwave radiometer gives an estimation of the LWP accurate to 100 mg cm-2. The shortwave cloud albedo was related to the LWPradiometer. The albedo increases with the LWP, independent of cloud type, when measured just above the cloud tops. The measured albedo is nearly the same as the calculated albedo when the LWPradiometer is larger than 60 mg cm-2 but much smaller than the calculated albedo when the LWPradiometer is less than 40 mg cm-2. Cloud-top irregularity is suggested to be the primary cause of this discrepancy. The degree of inhomogeneity of the horizontal distribution of liquid water appears to be correlated with the amount of precipitable water in the planetary boundary layer. -from Authors
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U2 - 10.1175/1520-0450-34.2.471
DO - 10.1175/1520-0450-34.2.471
M3 - Article
AN - SCOPUS:0028975186
SN - 0894-8763
VL - 34
SP - 471
EP - 481
JO - Journal of Applied Meteorology
JF - Journal of Applied Meteorology
IS - 2
ER -